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- The ocean floor has mountains including volcanoes, ridges, valleys, and plains1. It is entirely underlain by mafic oceanic crust, while the continental slopes are underlain by felsic continental crust2. The denser oceanic crust floats lower on the mantle than continental crust does, which is why oceans are oceans2. The study of ocean bottom features is called ocean floor topography, which includes the outer continental shelf, continental slopes, and ocean waves desktops3. The main features of the Pacific Ocean floor are the continental slopes, abyssal plains, volcanic seamounts and islands, and trenches at subduction zones4.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Bathymetry of the ocean floor showing the continental shelves oceanic plateaus (red), the mid-ocean ridges (yellow-green) and the abyssal plains (blue to purple). Like land terrain, the ocean floor has mountains including volcanoes, ridges, valleys, and plains.en.wikipedia.org/wiki/SeabedThe ocean floor is entirely underlain by mafic oceanic crust, while the continental slopes are underlain by felsic continental crust (mostly granitic and sedimentary rocks). Moreover, the denser oceanic crust floats lower on the mantle than continental crust does, which is why oceans are oceans.slcc.pressbooks.pub/physicalgeography/chapter/7-4/Ocean floor topography involves the study of ocean bottom features, including the outer continental shelf, continental slopes and ocean waves desktops.www.brighthubengineering.com/geotechnical-engin…The main features of the Pacific Ocean floor are the continental slopes, which drop from about 200 meters to several thousand meters over a distance of a few hundred kilometers, the abyssal plains—exceedingly flat and from 4,000 meters to 6,000 meters deep, volcanic seamounts and islands, and trenches at subduction zones that are up to 11,000 meters deep.openoregon.pressbooks.pub/earthscience/chapter/…
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